Tidal Effects on MFP Via the Intimate96 Test

Author(s):  
A. Tolstoy ◽  
S. Jesus ◽  
O. Rodriguez
Keyword(s):  
2021 ◽  
Vol 103 (4) ◽  
Author(s):  
Manuel Accettulli Huber ◽  
Andreas Brandhuber ◽  
Stefano De Angelis ◽  
Gabriele Travaglini

SPE Journal ◽  
2009 ◽  
Vol 14 (01) ◽  
pp. 144-152 ◽  
Author(s):  
Yong Zhao ◽  
Albert C. Reynolds
Keyword(s):  

2021 ◽  
Vol 89 (10) ◽  
pp. 909-915
Author(s):  
Ugo Besson
Keyword(s):  

The Copley Medal is awarded to Professor S. Chapman, F.R.S. Professor Chapman is distinguished for his contributions to many aspects of physics, astronomy and geophysics. His work on the kinetic theory of gases now forms the basis for much detailed study of gaseous phenomena, and over forty years ago his interest in these problems led him to consider the processes of diffusion and viscosity in stars. In addition to these important studies Chapman’s name has, for over half a century, been inseparably linked with problems in terrestrial magnetism and with a wide range of studies concerned with the high atmosphere, ionosphere and interplanetary space. From a statistical analysis of a great mass of data Chapman succeeded in demonstrating the existence of a small lunar component in the Earth’s quiet magnetic field variations, and he showed that the solar and lunar diurnal variations could be separated into a predominant component originating above the Earth’s surface and a subsidiary component within the Earth itself. From this standpoint he developed the general theory of the relation of the magnetic variations to the solar and lunar atmospheric tidal effects, a theory which has been fundamental to all subsequent work.


2011 ◽  
Vol 4 (2) ◽  
pp. 129-138 ◽  
Author(s):  
Mohd Ekhwan Toriman ◽  
Norbaya Hashim ◽  
Abd. Jalil Hassan ◽  
Mazlin Mokhtar ◽  
Hafizan Juahir ◽  
...  

2009 ◽  
Vol 5 (H15) ◽  
pp. 215-215 ◽  
Author(s):  
Sigrid Englich ◽  
Harald Schuh ◽  
Robert Weber

AbstractThe Earth rotation rate and consequently universal time (UT1) and length of day (LOD) are periodically affected by solid Earth tides and oceanic tides. Solid Earth tides induce changes with periods from around 5 days to 18.6 years, with the largest amplitudes occurring at fortnightly, monthly, semi-annual and annual periods, and at 18.6 years. The principal variations caused by oceanic tides have diurnal and semi-diurnal periods. For the investigation of the tidal effects with periods of up to 35 days, UT1 series are estimated from VLBI observation data of the time interval 1984–2008. The amplitudes and phases of the terms of interest are calculated and the results for diurnal and sub-diurnal periods are compared and evaluated with tidal variations derived from a GNSS-based LOD time series of 8 months. The observed tidal signals are finally compared to the predicted tidal variations according to recent geophysical models.


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